Chemistry Reference
In-Depth Information
Our discussion will be focused on the similarity of the cation arrays with the
which is implicit in it. Special emphasis will be given to the characteristics defining
each phase.
The differences between the cation arrays of both phases of FeLiPO
4
are simple.
As discussed above, triphylite FeLi[PO
4
] was described as a Fe-stuffed [Li
C
-Cl]
array of the NiAs type in which the P atoms (
-Cl) form a
hcp
array with all the
octahedral voids filled by the Li atoms (Fig.
5a
). Remember also that the pseudo-
structure of
C
-Li[ClO
4
] in triphylite showed a great distortion with respect to that
C
-FeLi[PO
4
], the octahedra of the
hcp
array of P atoms are now filled by the Fe atoms, forming so a Li-stuffed [FeP]
b
3.1 Relationships of
b
-FeLi[PO
4
] with Fe[SO
4
] and Li[ClO
4
]
If the EZKC [
4
] is applied to
-FeLiPO
4
, the structure can be rationalized by
assuming the one-electron transfer from the Li atom to the P atom which is
converted into a
b
C
-S. In this way,
b
-FeLiPO
4
should be formulated either as
Li
+
[FeP]
or as (
C
-He)[Fe
C
-S]. The result is that the cation array of the
b
-phase
would contain, in fact, a
-FeS substructure of the NiAs type [
25
]. In this
arrangement, the Li atoms are located in trigonal bipyramids, as the Fe atoms did
in triphylite. Consequently,
C
b
-FeLi[PO
4
] can then be formulated as a Li-stuffed
C
mcm, one sees that, once
O atoms are neglected, the FeS subarrays of both compounds are identical to the
high temperature phase of real FeS (also
C
C
C
-Fe[SO
4
]! The three
structures are shown in Fig.
9c, b and a
,
respectively.
The lack of similarity between the two phases, triphylite and
-FeLi[PO
4
],
in both figures). Although both drawings represent Li-stuffed NiAs-type struc-
tures, the important issue is that in
b
has formed a NiAs-type arrangement which is much more regular than that
although both structures are formed by an
hcp
array of PO
4
groups, the
chemical nature of the stuffing atoms (Fe and Li, respectively) seem to play a
decisive role in the formation of a “true” NiAs-type structure; that is, the
structure is close to the hexagonal regularity in
b
highly distorted in triphylite (Fig.
5a
). The reasons for these differences will be
discussed below.
b